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Most of the topography of the Bahama Banks is composed of calcium carbonate oolitic aragonite sand material.. Oolitic aragonite sand is composed of the calcium carbonate mineral, aragonite, with an egg-like shape ("oolitic" from the Ancient Greek word ᾠόν for "egg") and sand grain size.
The Bahamian dry forests are a tropical and subtropical dry broadleaf forest ecoregion in the Bahamas and the Turks and Caicos Islands, covering an area of 4,900 km 2 (1,900 sq mi). They are found on much of the northern Bahamas, including Andros , Abaco , and Grand Bahama , [ 1 ] where they are known as coppices. [ 2 ]
The geology of the Bahamas has been researched since the mid-19th century. The islands include Aeolian sands and limestone built on the basement rock of the Florida-Bahamas Platform. The islands are used to infer sea levels based on the arrangement of reef deposits.
White Bahamians constitute the majority (81.95%) of the district of Spanish Wells, which is located on St. George's Cay and Russell Island, north of Eleuthera. [11] White Bahamians are also a significant minority in Long Island (18.07%) and the Abaco Islands (13.76%), in which several settlements and small cays are majority white. [12]
Modern ooids from a beach on Joulter Cays, The Bahamas, with 0.5 mm scale Ooids on the surface of a limestone; Carmel Formation (Middle Jurassic) of southern Utah Thin-section of calcitic ooids from an oolite within the Carmel Formation (Middle Jurassic) of southern Utah
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